Planned stereo pairs have suitable stereo convergence angles and illumination by design.
In addition to planned stereo pairs, the Pairendipity software can identify overlapping
HiRISE images that are serendipitously suitable for stereo processing and find stereo
pairs within the CTX dataset.
Planned HiRISE stereo pairs are listed in the “Stereo Pair List (CSV)” link below.
Since this list is based on produced stereo anaglyphs it also contains a few serendipitous
pairs that underwent special processing. Most serendipitous HiRISE stereo pairs are listed
in the “Pairendipity Stereo” link, while CTX stereo pairs are listed
in “Pairendipity CTX Stereo”.
Images taken close together in time minimize illumination and frost differences and are
especially useful (see the Delta-Days column in the Pairendipity files or difference
the orbit numbers in the image IDs in the Stereo Pair List file). Stereo pairs
with both images planned within the same 14-day (168-orbit) operations cycle are known as SPORCs.
Degradation of Old Crater Rim on Northwest Slope of Acheron Fossae: ESP_016873_2185 ESP_017018_2185 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.30 | 218. | -8.3 | 1.584 | 42.0 | 41.0 |
Aram Chaos: ESP_016750_1830 ESP_017172_1830 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.769 | 339. | 3.01 | -13.3 | 47.2 | 51.0 |
Collapse Features on Hrad Vallis Mudflow: ESP_016467_2155 ESP_016533_2155 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.13 | 141. | 0.42 | -15.9 | 41.1 | 42.4 |
Source Region for Branch of Auqakuh Vallis: ESP_016826_2080 ESP_016971_2080 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 27.47 | 62.7 | -7.7 | 5.246 | 41.4 | 40.6 |
Well-Preserved Crater in Margaritifer Terra: ESP_016407_1675 ESP_016763_1675 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.5 | 345. | -0.5 | 12.61 | 52.5 | 55.3 |
Possible Phyllosilicates in Her Desher Vallis: ESP_016527_1550 ESP_025032_1550 (Interval in Earth days: 663) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -24.8 | 311. | -6.8 | 7.004 | 62.1 | 56.3 |
Layered Deposits along Floor of Melas Chasma: ESP_016673_1700 ESP_017952_1700 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.67 | 284. | -5.2 | 5.092 | 53.8 | 59.7 |
Cone Field in Phlegra Dorsa: ESP_016334_2090 ESP_016479_2090 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 28.57 | 174. | -6.3 | 7.838 | 40.7 | 39.6 |
Contact Between Different Lava Types on Olympus Mons: ESP_016820_1950 ESP_017888_1950 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 14.85 | 227. | -1.4 | 13.61 | 43.2 | 45.7 |
Well-Preserved Impact Crater with Central Peak in Acidalia Planitia: ESP_016777_2175 ESP_016289_2175 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 37.17 | 320. | -17. | 5.433 | 42.8 | 41.5 |
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